The Mn deposits occur as vein and replacement types, the latter being of greatest economic importance. The deposits are believed to have been formed by supergene concentration of Mn deposited by hydrothermal solutions (Skiba, 1964).
References
- Skiba, W. J. (1964): Geological studies in southwest Viti Levu. I. Petrology of the principal rock types. II. The manganese deposits. Fiji, Geol. Surv. Dept., Mem. 1, 1-56.
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